WEBVTT

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The majority of life on the planet is based in a food chain which revolves around sunlight.

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But of course in the deep sea, there is no light. Once you go below 200 meters, light just disappears.

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That means there are no plants down in the deep ocean.

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So there is a food chain that operates completely independently.

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Instead of having sunlight being used as the primary form of energy, chemical energy is used.

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And that is from these chemical-rich fluids, such as methane and also hydrogen sulfide,

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that leak out of the seafloor from fissures that have been formed by tectonic activity.

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And instead of there being plants, there are bacteria which act as the primary producers,

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and they utilize this chemical energy in a process known as chemosynthesis rather than photosynthesis,

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which is pretty amazing.

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So in geologically active areas such as the Gulf of Mexico

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the hydrogen-rich fluid and gas can result in a number of unique and rare environments

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that can range from a small patch of blackened reduced sediment to cold seeps with extensive mussel beds.

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Once you see a cold seep, it's just booming with animals.

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There are thousands upon thousands of animals in some cases.

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And that's because they've got a really plentiful energy source.

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So those hydrocarbons seep out of the seafloor.

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The bacteria then use them and that bacteria, which is constantly being replaced once it's eaten.

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We've also located brine pools, which is where extremely dense and salty brine seeps out of the seafloor

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and forms a lake at the bottom of the ocean, which is just amazing.

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And additionally, we've seen asphalt seeps, where liquid asphalt was seen leaking from the seafloor as droplets.

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So in the Gulf of Mexico, seep communities tend to be dominated by tubeworms and also mussels,

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which are endemic to chemosynthetic habitats.

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They are foundation species.

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And that means that they are species that create habitat for other species.

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And those tinier species that can be found include shrimp, chitins, eelpout fish, squat lobsters, limpets, snails --

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the list goes on.

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These species live here because they can find easy sources of food. They can find shelter.

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And they can also find hard substrate to attach to.

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And additionally, you can also find larger predators drifting in opportunistically,

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such as large crabs, octopus, fish, and so on, that come in to have a quick meal and then go on their way.

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Further afield from these areas of seepage, there can be hard substrates in the form of asphalt concretions or authegenic carbonates.

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And in those areas, we can find corals and other suspension feeding animals using the hard substrate to anchor to

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but also to get them up into the water column.

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So we're exploring for chemosynthetic habitats for a number of reasons.

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First of all, they are insanely cool and why would you not?

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Secondly, they provide us with many ecological services,

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which a lot of people don't actually realize.

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They likely have a role in nutrient cycling in our world's oceans.

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They enhance fisheries.

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And of course collecting this kind of critical baseline information about these vulnerable habitats

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will allow more effective management of the Gulf of Mexico deep seafloor.

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And lastly, they inspire people. They provide us with a sense of awe, and that's something that really shouldn't be underestimated.

